Seismic imaging of the Main Frontal Thrust in Nepal reveals a shallow décollement and blind thrusting
Because great earthquakes in the Himalaya have an average recurrence interval exceeding 500 yr, most of what we know about past earthquakes comes from paleoseismology and tectonic geomorphology studies of the youngest fault system there, the Main Frontal Thrust (MFT). However, these data are sparse...
Saved in:
Main Authors: | Almeida, Rafael V., Hubbard, Judith, Liberty, Lee, Foster, Anna, Sapkota, Soma Nath |
---|---|
Other Authors: | Asian School of the Environment |
Format: | Article |
Language: | English |
Published: |
2019
|
Subjects: | |
Online Access: | https://hdl.handle.net/10356/88640 http://hdl.handle.net/10220/50459 |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Institution: | Nanyang Technological University |
Language: | English |
Similar Items
-
Fluvial sedimentary response to late quaternary climate and tectonics at the Himalayan frontal thrust, Central Nepal
by: Hamahashi, Mari, et al.
Published: (2023) -
Physics-based scenario of earthquake cycles on the Ventura Thrust system, California : the effect of variable friction and fault geometry
by: Ong, Miranda Su Qing, et al.
Published: (2019) -
Estimating the return times of great Himalayan earthquakes in eastern Nepal : evidence from the Patu and Bardibas strands of the main frontal thrust
by: Bollinger, L., et al.
Published: (2015) -
Structural segmentation controlled the 2015 Mw 7.8 Gorkha earthquake rupture in Nepal
by: Hubbard, Judith, et al.
Published: (2019) -
Constraints on the shallow deformation around the Main Frontal Thrust in central Nepal from refraction velocities
by: Liu, Yixiang, et al.
Published: (2020)